The response of the climate system to astronomical parameters is an important scientific issue, but the internal processes and feedbacks need to be better understood. This study investigates the differences of the climate response to the astronomical forcing between the Northern (NH) and Southern (SH) hemispheres based on a more than 90,000-year long transient simulation using the model LOVECLIM. The astronomical parameters of the period 511–417 ka BP covering MIS-13, MIS-12 and MIS-11 are used, and greenhouse gases (GHG) concentrations and ice sheets are fixed, in order to investigate the role of insolation alone. Our results show that the response of sea ice and sea surface temperature (SST) to precession and obliquity is different betwee...
Five paired global climate model experiments, one with an ice pack that only responds thermodynamica...
Five paired global climate model experiments, one with an ice pack that only responds thermodynamica...
Idealized atmosphere-only simulations with reduced and removed Arctic sea-ice cover and increased Ar...
The response of the climate system to astronomical parameters is an important scientific issue, but ...
The climate response of different latitudes in both Northern (NH) and Southern (SH) Hemispheres to t...
The response of climate system to astronomical parameters is a very important scientific issue, but ...
The response of the climate system to astronomical parameters, greenhouse gases (GHG) and ice sheets...
The climate of the nine interglacials of the past 800,000 years has been simulated with both snapsho...
Understanding the variations of water cycle on orbital timescale and their response to astronomical ...
We combine reconstructions, climate model simulations and a conceptual model of glacial climate chan...
The climate of nine interglacials of the past 800,000 years has been simulated with both snapshot an...
Understanding the sea ice variability and the mechanisms involved during warm periods of the Earth i...
Understanding the sea ice variability and the mechanisms involved during warm periods of the Earth i...
The climate of nine interglacials of the past 800,000 years has been simulated with both snapshot an...
Understanding the sea ice variability and the mechanisms involved during warm periods of the Earth i...
Five paired global climate model experiments, one with an ice pack that only responds thermodynamica...
Five paired global climate model experiments, one with an ice pack that only responds thermodynamica...
Idealized atmosphere-only simulations with reduced and removed Arctic sea-ice cover and increased Ar...
The response of the climate system to astronomical parameters is an important scientific issue, but ...
The climate response of different latitudes in both Northern (NH) and Southern (SH) Hemispheres to t...
The response of climate system to astronomical parameters is a very important scientific issue, but ...
The response of the climate system to astronomical parameters, greenhouse gases (GHG) and ice sheets...
The climate of the nine interglacials of the past 800,000 years has been simulated with both snapsho...
Understanding the variations of water cycle on orbital timescale and their response to astronomical ...
We combine reconstructions, climate model simulations and a conceptual model of glacial climate chan...
The climate of nine interglacials of the past 800,000 years has been simulated with both snapshot an...
Understanding the sea ice variability and the mechanisms involved during warm periods of the Earth i...
Understanding the sea ice variability and the mechanisms involved during warm periods of the Earth i...
The climate of nine interglacials of the past 800,000 years has been simulated with both snapshot an...
Understanding the sea ice variability and the mechanisms involved during warm periods of the Earth i...
Five paired global climate model experiments, one with an ice pack that only responds thermodynamica...
Five paired global climate model experiments, one with an ice pack that only responds thermodynamica...
Idealized atmosphere-only simulations with reduced and removed Arctic sea-ice cover and increased Ar...